4_Moss_animals_of_the_Dutch_part_of_the_North_Sea_and_coastal_waters_of_the_Netherlands_Bryozoa www.researchgate.net/publication/297380674_Moss_animals_of_the_Dutch_part_of_the_North_Sea_and_c [...] oastal_waters_of_the_Netherlands_Bryozoa www.researchgate.net/publication/297380674_Moss_animals_of_the_Dutch_part_of_the_North_Sea_and_coastal_waters_of_the_Netherlands_Bryozoa www.re [...] researchgate.net/publication/297380674_Moss_animals_of_the_Dutch_part_of_the_North_Sea_and_coastal_waters_of_the_Netherlands_Bryozoa 109 Bugula neritina* (Linnaeus, 1758) Eine bäumchenförmig wachsende Bryozoe

insights into the carbon storage potential in the German oceans in the future. In the third part, the status of climate change effects in the German North Sea and Baltic Sea, as well as the impact of climate [...] marine ecosystems, and the seafloor is referred to as Blue carbon. This study presents the results of a literature review on published data related to the Blue carbon potential of different ecosystems and [...] biotopes along the German coasts and within the German EEZ as well as on climate change impacts on these. The focus lies on salt marshes and seagrass beds, as well as the possible potential of macroalgae,

refers to the organic carbon content stored in the sediment of marine and coastal ecosystems. Against the backdrop of the current climate and biodiversity crisis, the Blue Carbon potential of marine ecosystems [...] researched and discussed. A study by the German Federal Agency for Nature Conservation (BfN) summarises the current state of knowledge on the Blue Carbon potential of the German North and Baltic Seas. Seagrass [...] review of coastal ecosystem services in the Baltic Sea. Science of the Total Environment 755: e142565. DOI: 10.1016/j. scitotenv.2020.142565 HELCOM/Helsinki Commission (2021a): Report of the HELCOM workshop

not really the true definition of PFTs. However, in the scope of our project the limitation of satellite products was clear, therefore we still use the term PFT. In chapter any grouping of phytoplankton [...] wrote after the meeting the first draft of the document. Then it has been circulated with two iterations among the writing team, LOV and PML as part of the SynSenPFT consortium, and the “PFT algorithm i [...] limitation of this modelling approach is the choosing of the parameters governing the growth and loss of PFTs in the model. For instance laboratory studies have found maximum growth rates of different diatom

concern for the safety. Furtherm ore, the area of the scientific activities is increasing, inside the islands and on the sea, w hich requires a m ajor effort for the w eather forecaster to study the w eather [...] eather of other areas w e are not fam iliar. This im ply also the know ledge of w eather in-situ. The activities on the sea (sam pling of m arine flora and w ildlife) are increasing m ore and m ore in the last [...] ith resolutions of 10’s to 100’s of m eters. Forecasting is the greatest challenge and identified need. H igh quality observations are required to better understand the base state of the ice environm ent

quence of the dependency of nutrients and light, the concentration of Chl-a in the Arctic Ocean is seasonal (Fig. 1.1), since the availability of these are driven by the sea-ice cover dynamics, the seasonal [...] understanding the typical size of the errors. Coefficient of Determination (R2) The coefficient of determination, R2, is a statistical measure that indicates the proportion of the variance in the dependent [...] measures of water clarity and light penetration. The presence of phytoplankton contributes to the light attenuation in the upper ocean layers, affecting the value of KD490. The ZSD is a simple measure of water

absorption coefficient (aph) or the total absorption coefficient (a). The method is based on the knowledge that 80% of the variability in the shape of the aph normalized by its spectral mean from 400 – [...] SynsenPFT. The advantage of the second method is that the relationship can be applied to OC-PFT grid cells even in the absence of PhytoDOAS data, increasing the spatial coverage of the SynsenPFT. Sy-4SciPFT-RB-D1 [...] will adapt the parameterisation relating the fit factor of the specific phytoplankton absorption spectrum divided by the penetration depth with the "real" Chla of the phytoplankton type. The PFT signal

we first identified the peak Chla of the time series and then looked backwards in time to find the start of the bloom (Brody et al. , 2013). The end of the bloom was determined as the first week when Chla [...] Gaps in the plots indicate that the corresponding phenological indexice could not be calculated because, the peak of the bloom was in the first or last month of the period investigated or the Chla did not [...] values below the threshold. Both issues avoid the estimation of the start, end and duration of the bloom. Figures 40 to 43 present the estimated start, peak, end and total duration of the dia- SynSenPFT

esa-oceancolour-cci.org/ 3 the Journal , which will highlight the major scientific results presented at the workshop. Each section of the report, dealing with one of the themes of the workshop, is self-contained [...] better the needs of the user community in general and the modelling community in particular? What should be done to ensure the continuity of the data into the foreseeable future and to ensure that the quality [...] duplication of efforts. The presentations in the session on “Ocean-Colour Applications for Climate Studies” gave a broad idea of the state of the art. The invited talk by Brian Franz described the NASA activities

esa-oceancolour-cci.org/ 3 the Journal , which will highlight the major scientific results presented at the workshop. Each section of the report, dealing with one of the themes of the workshop, is self-contained [...] better the needs of the user community in general and the modelling community in particular? What should be done to ensure the continuity of the data into the foreseeable future and to ensure that the quality [...] duplication of efforts. The presentations in the session on “Ocean-Colour Applications for Climate Studies” gave a broad idea of the state of the art. The invited talk by Brian Franz described the NASA activities